Multi-decadal sea level trends and land movements in the Mediterranean Sea with estimates of factors perturbing tide gauge data and cumulative uncertainties
Multi-decadal sea level trends and land movements in the Mediterranean Sea with estimates of factors perturbing tide gauge data and cumulative uncertainties
Sea level trends in the Mediterranean Sea and their forcing parameters are explored. Multi-decadal trends from available tide gauge records are estimated together with the contribution of the oceanic (steric and mass variations) and atmospheric (pressure and wind) changes as well as land movements (including GIA). Each forcing factor is considered as an independent process creating its own signal on a tide gauge, and subject to uncertainties of measurement, deduction or interpretation of proxy data for that factor. The paper is focused on the uncertainty of the estimate of each forcing factor, including the estimate of the eustatic part affecting the Mediterranean Sea, obtained by subtracting GIA and land movements obtained from geomorphological and archaeological data at the tide gauge stations.
sea level, tide gauge, mediterranean, steric sea level, gia, land movements, archaeological data, geomorphology
63-76
Tsimplis, M.
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Spada, G.
f61e22ac-80c2-4bda-b29e-9f5733ae6e15
Marcos, M.
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Flemming, N.
ca15a04a-9b7c-4b59-8f50-f568b49d6fae
March 2011
Tsimplis, M.
df6dd749-cda4-46ec-983c-bf022d737031
Spada, G.
f61e22ac-80c2-4bda-b29e-9f5733ae6e15
Marcos, M.
3cd7a6cd-def3-47a9-a7c4-7ef305fc0bf1
Flemming, N.
ca15a04a-9b7c-4b59-8f50-f568b49d6fae
Tsimplis, M., Spada, G., Marcos, M. and Flemming, N.
(2011)
Multi-decadal sea level trends and land movements in the Mediterranean Sea with estimates of factors perturbing tide gauge data and cumulative uncertainties.
Global and Planetary Change, 76 (1-2), .
(doi:10.1016/j.gloplacha.2010.12.002).
Abstract
Sea level trends in the Mediterranean Sea and their forcing parameters are explored. Multi-decadal trends from available tide gauge records are estimated together with the contribution of the oceanic (steric and mass variations) and atmospheric (pressure and wind) changes as well as land movements (including GIA). Each forcing factor is considered as an independent process creating its own signal on a tide gauge, and subject to uncertainties of measurement, deduction or interpretation of proxy data for that factor. The paper is focused on the uncertainty of the estimate of each forcing factor, including the estimate of the eustatic part affecting the Mediterranean Sea, obtained by subtracting GIA and land movements obtained from geomorphological and archaeological data at the tide gauge stations.
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Published date: March 2011
Keywords:
sea level, tide gauge, mediterranean, steric sea level, gia, land movements, archaeological data, geomorphology
Organisations:
National Oceanography Centre,Southampton, Marine Physics and Ocean Climate
Identifiers
Local EPrints ID: 178107
URI: http://eprints.soton.ac.uk/id/eprint/178107
ISSN: 0921-8181
PURE UUID: 6e6c773c-b7a5-4b3f-9511-1e7008505e74
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Date deposited: 22 Mar 2011 16:40
Last modified: 14 Mar 2024 02:44
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Contributors
Author:
M. Tsimplis
Author:
G. Spada
Author:
M. Marcos
Author:
N. Flemming
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